ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
全新世以来太行山前倾斜平原地下水演化规律
  
关键词:Holocene  groundwater  recharge period  evolution of hydrologic cycle  piedmont clinoplain of Taihang mountains
基金项目:河海大学博士后基金课题,国土资源部重点基础项目(9501110 ),国土资源部百名科技人才基金资助课题
作者单位
张光辉 国土资源部环境地质开放研究实验室,石家庄 
费宇红 中国地质科学院水文地质工程地质研究所,河北正定 
聂振龙 中国地质科学院水文地质工程地质研究所,河北正定 
李惠娣 中国地质科学院水文地质工程地质研究所,河北正定 
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摘要:
The Evolution Regularity of Groundwater in Piedmont Clinoplain of Taihang Mountains since Holocene
      The formation and the evolution of regional groundwater have been closely related to periodic hydrological cycle in piedmont clinoplain of Taihang mountains since Holocene.The main recharge period of groundwater was 8.0 to 3.5 ka B.P.,during which the recharge of groundwater was sufficient.This lay the foundation of present groundwater system.
ZHANG Huang-hui,FEI Yu-hong,NIE Zhen-long,LI Hui-di.2000.The Evolution Regularity of Groundwater in Piedmont Clinoplain of Taihang Mountains since Holocene[J].Acta Geoscientica Sinica,21(2):121-127.
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